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Associations between redox‐sensitive trace metals and microbial communities in a Proterozoic ocean analogue

Abstract.

"Constraints on Precambrian ocean chemistry are dependent upon sediment geochemistry. However, diagenesis and metamorphism can destroy primary biosignatures, making it difficult to consider biology when interpreting geochemical data. Modern analogues for ancient ecosystems can be useful tools for identifying how sediment geochemistry records an active biosphere. The Middle Island Sinkhole (MIS) in Lake Huron is an analogue for shallow Proterozoic waters due to its low oxygen water chemistry and microbial communities that exhibit diverse metabolic functions at the sediment–water interface. [...]"

Source: Geobiology
Authors: Kathryn I. Rico
DOI: 10.1111/gbi.12388

Read the full article here.